What is Rock?
Rocks ordinarily lie everywhere on the ground of the Earth. They constitute most of the landforms, as we often notice. For instance, rocks make up the mountains and most of the non-water portions of the earth’s surface. A rock is hence defined as a solid naturally occurring mass of consolidated mineral matter. This is because rocks are made up of granules of different minerals that form bigger and hard masses.
In simple terms, a rock is made up of two or more minerals and can also contain organic compounds. Rocks occur in different shapes, colors, weights, strengths, sizes, and texture. Rocks also change from one form to another and differ from one region to another because of the rock cycle. These changes usually take thousands or millions of years. Rocks are also mainly porous or non-porous in nature.
National Geographic defines rock as,
“To geologists, a rock is a natural substance composed of solid crystals of different minerals that have been fused together into a solid lump. The minerals may or may not have been formed at the same time. What matters is that natural processes glued them all together.”
Table of Contents
What are Various Types of Rocks?
Rocks formation takes different processes. Their formations are classified according to the rock types since the processes involved normally results in a characteristic relationship between the mineral grains. Rock formations, therefore, are in three basic groups which include igneous, sedimentary, and metamorphic.
1. Igneous Rocks
Igneous rocks form from the cooling of magma – molten materials in the earth’s crust. From the terminology itself, igneous means from fire or heat. Molten materials are found below the earth crust and are normally subjected to extreme pressure and temperatures – up to 1200° Celsius. Because of the extreme heat levels, igneous rocks do not contain organic matter or fossils.
The molten minerals interlock and crystallize as the melt cools and form solid materials. In the long-run, the melt forms a cool hard rock made up of crystals with no open spaces and don’t exhibit any desirable grain alignment. The rocks may be made up entirely of one mineral or various minerals, and their sizes are determined by the cooling process.
Igneous rocks are of two types, intrusive and extrusive. Intrusive igneous rocks are formed when the magma cools off slowly under the earth’s crust and hardens into rocks. Gabbro and granite are examples of intrusive igneous rocks. Rapid cooling results in smaller crystals while slow cooling results in large crystals. Intrusive rocks are very hard in nature and are often coarse-grained.
They are also sometimes referred to as plutonic rocks. On the other hand, extrusive rocks are formed when molten magma spill over to the surface as a result of volcanic eruption. The magma on the surface (lava) cools faster on the surface to form igneous rocks that are fine grained. Examples of such kind of rocks include pumice, basalt, or obsidian.
2. Sedimentary Rocks
Sedimentary rocks are secondary formed materials since they are made up from the buildup of weathered and eroded pre-existing rocks. In precise, sedimentary rocks are formed from sediment deposits. Every rock grain initially separated from other rocks. Tiny debris from rock masses and eroded mountains together with soils, sand, and other granite pieces are normally washed from highlands to low areas.
After many years, these materials finally settle down through the process of sedimentation. Some may accumulate under water and others on the lower areas of the land. As the materials move, they are smoothened and rounded by abrasion, and they settle down by leaving pore spaces between the grains which make them achieve their distorted shape.
The compaction effect due to the weight of the piling layers of materials reduces the porosity of the rocks formed and intensifies the cohesion between the grains. At times, fossil fuels and organic matter may settle within the sediments leading to cementation.
Cementation is the gluing of the rock pieces together either by salt compounds or organic matter. When these materials eventually harden, they produce sedimentary rocks. Examples of sedimentary rocks include mudstone, limestone, sandstone, and conglomerate.
3. Metamorphic Rocks
Metamorphic rocks form out of other rocks. They are predominantly sedimentary or igneous rocks that have undergone changes as a result of extreme pressure and heat. The name defines the formation whereby ‘meta’ means change and ‘morph’ means ‘form.’ Large tectonic movements and magma intrusions create earth movements and subsequently cause the rocks to move and shift.
In turn, the movements subject other rocks to extreme pressure and heat which contributes to changes and assemblage of some minerals. The changes typically modify the rock’s crystal type and sizes and may also subject the rocks to further radical changes. Metamorphic processes come about at heats between 150° and 795° Celsius.
The heat from magma and the heat from friction along fault lines is the major contributor of heat that brings about the rock changes. Even though the rocks do not actually melt, some mineral groupings redistribute the elements within the original minerals to form new forms of minerals that are more stable at the new temperatures and pressures. As a result, the original rocks are transformed into metamorphic rocks.
Metamorphic rocks formed from direct magma heating and intrusions are termed as thermal or contact metamorphic rocks. Those formed as a result of widely distributed pressure and temperature changes induced by tectonic movements are known as regional metamorphic rocks. Examples of metamorphic rocks include marble formed from limestone and slate formed from shale.
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